The nondimensional volumetric flux of this quantity is proportional to the three-halves power of boundary shear stress minus critical boundary shear stress. Those relations were improved by employing a "hiding function" by Wilcock and Crowe. A conservation of mass equation that often includes a subsidence term that applies to its transport is called the Exner equation. It may be entrained in different manners according to the value of the Rouse number. One form of this material forms paha and greda ridges and is called loess, and its deposition can form mouth bars and oxbow lakes, the former of which creates distribut
The nondimensional volumetric flux of this quantity is proportional to the three-halves power of boundary shear stress minus critical boundary shear stress. Those relations were improved by employing a "hiding function" by Wilcock and Crowe. A conservation of mass equation that often includes a subsidence term that applies to its transport is called the Exner equation. It may be entrained in different manners according to the value of the Rouse number. One form of this material forms paha and greda ridges and is called loess, and its deposition can form mouth bars and oxbow lakes, the former of which creates distributary networks at river deltas. This material can be transported through saltation as part of the bed load. For 10 points, name this material transported by rivers whose buildup and compression forms a namesake kind of rock.
The nondimensional volumetric flux of this quantity is proportional to the three-halves power of boundary shear stress minus critical boundary shear stress.
{sediment}